Table 2 Input parameters for the MOLASSES lava flow modelling for three DEVORA scenarios. Coordinates are provided in New Zealand Transverse Mercator (2000)
From: The influence of surficial features in lava flow modelling
Parameter | Scenario | Value | Source/Justification |
|---|---|---|---|
Easting (M) | Mt Eden | 1,757,370 | Hayes et al. (2018) |
Ōtāhuhu | 1,765,010 | ||
Birkenhead Lava Flow 1 | 1,755,916 | ||
Birkenhead Lava Flow 2 | 1,755,914 | ||
Northing (M) | Mt Eden | 5,916,250 | |
Ōtāhuhu | 5,909,090 | ||
Birkenhead Lava Flow 1 | 5,923,738 | ||
Birkenhead Lava Flow 2 | 5,923,767 | ||
Volume (M3) | Mt Eden | 59,871,290 | |
Ōtāhuhu | 450,970 | ||
Birkenhead Lava Flow 1 | 960,810 | ||
Birkenhead Lava Flow 2 | 8,647,290 | ||
Modal thickness (M) | all | 17.5 | Hayes et al. (2018) |
Pulse Volume (M3) | Mt Eden | 1000 | Based on authors’ available computational memory |
Ōtāhuhu | 10 | ||
Birkenhead Lava Flow 1 | 10 | ||
Birkenhead Lava Flow 2 | 100 |